Atmospheric oscillations over the last millennium

The variations of global atmospheric oscillations over the last millennium, including the North Atlantic scillation (NAO), the North Pacific Oscillation (NPO) highly associated with the Pacific Decadal Oscillation (PDO), the Southern Oscillation (SO) and the Antarctic Oscillation (AAO), are studied...

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Bibliographic Details
Published in:Chinese Science Bulletin
Main Authors: Huang JianBin, Wang ShaoWu, Gong DaoYi, Zhou TianJun, Wen XinYu, Zhang ZiYin, Zhu JinHong
Other Authors: Huang, JB (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China., Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China., Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Coll Resources Sci & Technol, Beijing 100875, Peoples R China., Chinese Acad Sci, Inst Atmospher Phys, LASG, Beijing 100871, Peoples R China.
Format: Journal/Newspaper
Language:English
Published: 科学通报 英文版 2010
Subjects:
atmospheric oscillation
climate variability
ENSO
Medieval Warm Period
Little Ice Age
PACIFIC DECADAL OSCILLATION
SOUTHERN ANNULAR MODE
VARIABILITY
PATAGONIA
TELECONNECTIONS
WINTER
INDEX
Antarctic
Pacific
Patagonia
The Antarctic
Antarc*
North Atlantic
Online Access:https://hdl.handle.net/20.500.11897/148673
https://doi.org/10.1007/s11434-010-3210-8
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Summary:The variations of global atmospheric oscillations over the last millennium, including the North Atlantic scillation (NAO), the North Pacific Oscillation (NPO) highly associated with the Pacific Decadal Oscillation (PDO), the Southern Oscillation (SO) and the Antarctic Oscillation (AAO), are studied and compared in this paper based on observations and reconstructed data. The cross correlation analysis of AAO, NAO and NPO shows that there is no significant relationship on interannual variation among them. However, the consistency on decadal variability is prominent. During A.D.1920-1940 and A.D.1980-2000, the positive (strong) phase was dominant and the negative (weak) one noticeable during A.D.1940-1980. In addition, the reconstructed atmospheric oscillations series demonstrate that the positive phase existed in the early of the last millennium for NAO and in the late of the last millennium for AAO, respectively; while it occurred in the mid-late of the last millennium for PDO and ENSO. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000280808100021&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Multidisciplinary Sciences SCI(E) 3 ARTICLE 22 2469-2472 55

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